TY - JOUR
T1 - Prediction of the stability of the rhombohedral phase in IV-VI monochalcogenides and its origin
AU - Argaman, Uri
AU - Abutbul, Ran E.
AU - Segev, Elad
AU - Makov, Guy
N1 - Publisher Copyright:
© 2017 The Royal Society of Chemistry.
PY - 2017/1/1
Y1 - 2017/1/1
N2 - The rhombohedral monotellurides, GeTe and SnTe, are non-centrosymmetric materials with ferroelectric behavior and potential applications in thermoelectricity and spintronics. In a previous computational study [E. Segev, U. Argaman, R. E. Abutbul, Y. Golan and G. Makov, CrystEngComm, 2017, 19, 1751-1761], it was found that the rhombohedral phase may also be the thermodynamically most stable phase in SnSe and GeSe at low temperatures. In the present study, we explore the mechanical and thermodynamic stability of the rhombohedral phase in these systems and its enhancement as a function of pressure and temperature using density functional theory calculations. Within the region of stability, we examine the structure, bonding and physical properties of the rhombohedral phase. This phase is a distorted rock-salt phase forming a non-spherical lone-pair with an opposite directionality to the chemical bond. The monochalcogenides in this phase exhibit ferroelectric behavior, and we calculate the electric polarization. Finally, the transition from a rhombohedral to rock-salt phase at high pressures is examined and found to be second-order at zero Kelvin.
AB - The rhombohedral monotellurides, GeTe and SnTe, are non-centrosymmetric materials with ferroelectric behavior and potential applications in thermoelectricity and spintronics. In a previous computational study [E. Segev, U. Argaman, R. E. Abutbul, Y. Golan and G. Makov, CrystEngComm, 2017, 19, 1751-1761], it was found that the rhombohedral phase may also be the thermodynamically most stable phase in SnSe and GeSe at low temperatures. In the present study, we explore the mechanical and thermodynamic stability of the rhombohedral phase in these systems and its enhancement as a function of pressure and temperature using density functional theory calculations. Within the region of stability, we examine the structure, bonding and physical properties of the rhombohedral phase. This phase is a distorted rock-salt phase forming a non-spherical lone-pair with an opposite directionality to the chemical bond. The monochalcogenides in this phase exhibit ferroelectric behavior, and we calculate the electric polarization. Finally, the transition from a rhombohedral to rock-salt phase at high pressures is examined and found to be second-order at zero Kelvin.
UR - http://www.scopus.com/inward/record.url?scp=85032257020&partnerID=8YFLogxK
U2 - 10.1039/c7ce01374d
DO - 10.1039/c7ce01374d
M3 - Article
AN - SCOPUS:85032257020
SN - 1466-8033
VL - 19
SP - 6107
EP - 6115
JO - CrystEngComm
JF - CrystEngComm
IS - 41
ER -